Изображения страниц
PDF
EPUB

Nov. 7, 1872]

NATURE

many valuable papers were read, followed by fruitful discussions; a final general meeting to listen to something that would interest all, and then the dispersion. This Society appears to be satisfactorily accomplishing its professed aim of increasing the interests of the people generally in scientific studies, of establishing intimate and familiar relations between men of science engaged upon the same subject, and of fostering a harmonious spirit of labour all over the country. We give an abstract of the report contained in the Bibliothèque Universelle.

Prof. Volpicelli gave a paper on Atmospheric Electricity and the best method of studying it. Having made experiments, in calm weather, according to the methods both of Franklin and of Peltier (in the former of which a fixed uninsulated rod is used, connected with an electrometer by a wire, while in the latter a moveable metallic point with similar connection is sent up into the atmosphere), he found the results always contradictory as regards the quantity, and sometimes also as regards the quality, of electricity indicated.

On all the days in which the air was not much agitated, the time and circumstances being the same, the moving rod gave a greater quantity of electricity than the fixed; and the former often showed positive electricity, while the latter showed negative.

It has been shown that the earth is a body negatively electrified. It follows that any conducting substance is electrified positively when it rises in the atmosphere, and becomes negative, on the other hand, as it descends. The indications of the metallic rod shot into the air are therefore modified by the influence of the earth, and do not give a means of determining the electricity of the surFranklin's fixed rod, on the other rounding atmosphere. hand, is free from these disturbing influences.

That a conductor gives positive electricity as it rises in the atmosphere, and negative as it descends, may be proved by experiment. Suppose, e.g., the fixed rod gives negative electricity; if a flame be applied to the point of it, the apparatus will indicate positive electricity. The flame produces an upward current of air, which, by its motion, and under the influence of the earth, gives a neutralising positive electricity, so that the point of the fixed rod becomes positively charged. (It is necessary that the flame should have a high calorific power.)

If the flame be now brought down to the ground, one or other of three effects will occur:-if the flame is not very strong, negative electricity will be indicated; if somewhat hotter, there will be no electricity at all; if very intense, the electricity will be positive. These effects are readily explained as the resultants of two opposing actions, the production of positive electricity by the ascending current of air, and the production of negative through the influence of the earth on the descending flame. The general inference Prof. Volpicelli draws is the preferability of Franklin's method to the other.

M. Müller, professor at Fribourg, gave an account of experiments on the lower Glacier of the Grindelwald, with reference to the optical properties of glacial ice. His experiments partly confirm the results obtained by MM. Grad and Dupré, that thin lamella of ice cut horizontally at the base of the glacier, give, in Norremberg's apparatus, systems of coloured rings with a dark cross. This property, morcover, appears only at certain separate parts of the lamella, and the system of rings is always more or less incomplete, which is sufficiently explained by the irregular structure of the ice of glaciers, in which, necessarily, there are only distant traces of the mode of original formation. Vertical sections gave no coloured rings.

M. Louis Dufour described some important researches on the Diffusion of Gases across diaphragms and the variations of temperature accompanying it. He studied the cases (among others) of hydrogen and air, of air and carbonic acid.

He distinguishes the diffusion at constant pressure, and
the diffusion with change of pressure. The porous vessel
very sensitive thermometer, and is enclosed in another
containing the gas with slower diffusion contains also a
vessel, in which the other gas circulates. A glass tube,
passing through the stopper of the porous vessel, can be
put in communication either with external air (pressure
constant) or with a manometer. The whole is enclosed
with a cathetometer.
in an envelope of cotton. The thermometer is observed

1. Diffusion at constant pressure.-First of all, taking
as example hydrogen and air, equilibrium of temperature
and that inside; then hydrogen is made to circulate, and
is established between the air outside of the porous vessel
it is seen that the thermometer in the interior falls. A
a rise of temperature on the side of the entering gas,
large number of experiments showed that there is always
and a fall of temperature on the side of the escaping gas.
take place throughout the gaseous mass, but only at the
He conceives that at the part
M. Dufour believes this change of temperature does not
surface of the diaphragm.
where the gas enters there is condensation and compres-
sion, causing development of heat. In the opposite case
there is expansion of the gas, and hence absorption of

heat.

2. Diffusion with change of pressure. In this case the phenomenon is complicated by variations in the temperature according to the pressure. When the diffusing gas enters the porous vessel, the thermometer indicates first a slight rise of temperature resulting from rapid increase of pressure; it then falls, and to a much greater extent (of a degree e.g.) commences again to rise gradually, falls a little again, in consequence of the escape of the other gas and the rarefaction produced; then continually rises. The effects are represented by a curve.

M. Dufour also studied the case of diffusion between He observed there was dry air and moist air. different degrees of humidity; and, contrary to what always diffusion between two quantities of air having one might expect from Graham's law (the vapour of water being lighter than air), the diffusion takes place The diffusion is readily from the dry to the humid." The laws of variation of served in the case of two gases. temperature in this case conform to what M. Dufour ob

indicated by a water manometer, and M. Dufour thinks the principle might be applied in hygrometry. It is evident that the general principle must have numerous applications in the organic world. M. Reichert described a thermo-regulator, in which the mercury of a thermometer to a certain point, the passage of the heat-producing which was placed in a heated liquid interrupted, on rising gas.

M. Mousson described a method for measuring the dispersion in the different parts of the spectrum furnished by a prism or any spectroscope whatever. The dispersion The law obtained with a prism, it is believed much less rapidly in varies, it is known, in the different portions of the spectrum the red, much more rapidly in the violet. M. according to which it varies changes according to the different prisms and different substances used. Mousson proposes a new simple process by means of which the law can be directly determined for each spectroscope. It consists in observing with the spectroscope the spectrum given by a network (réseau) of diffraction, of which the lines ought to be perpendicular if the edges of the prism are horizontal. There is thus sentation of the law sought. obtained a curved spectrum, which is the graphic repre

Other papers in the section were by M. de la Rive on the influence of a magnet, and particularly upon the mechanical rotation of the electric discharge in rarified gases under the M. E. Hagenbach expounded the principal action which this discharge could exercise in its rotating results of his beautiful researches upon Fluorescence:

movement.

and M. Volpicelli concluded the work of the section by a communication on Electrostatic Induction.

Geology is the branch of Natural History which is most cultivated in Switzerland. Notwithstanding its small extent, that country has the most varied field for observation in the mountain-chains of the Jura and the Alps; there are few important questions whose solution cannot be found in these mountains; and many Swiss names are found among those who have done most to advance that science. During the last year geological studies have received a great impulse in Switzerland by the subsidies which the Confederation vote for that purpose; each year the State grants a sum in aid of the researches of a certain number of geologists, and for the study of a new part of the territory. The works which result are published under the care of a special commissioner of the Society of Natural Science. As might be expected then, the Geological Section was very numerously attended, and the papers read on the subject were many and valuable. We learn from M. A. Fauzes' general lecture that the Society have taken similar steps for the study and preservation of Swiss boulders to those taken by the Royal Society of Scotland, whose report we gave in a recent number.

M. V. Gross brought under the notice of the members a series of objects belonging to the lacustrine, dwellings of the Lake of Bienne, worthy of the attention even of those who have seen the richest collections of this kind. There was the bit of a bridle almost complete belonging to the station of Mörigen, which belongs to the age of bronze; at the present time only one similar fragment is known. Incrustations of iron upon a bronze knife tend to confirm what has already been conjectured, that at the first appearance of iron it was regarded as a most precious metal. The station of Lüschersz, of the stone age, has been discovered by M. Gross, and has furnished axes of nephrite and jade of a size not hitherto met with in lacustrine dwellings. It is known that these rocks are not found in Europe; and it is a question whether these lake-dwellers obtained them by commercial intercourse with Asia, or whether these rare articles were preserved as heirlooms in families from the period of their emigration from their ancient Asiatic home.

M. Ch. Vogt communicated to the section the results of his microscopic study of rocks. One of the questions which he wished to resolve is whether the microscope can enable us to know whether or not a rock has ever been in an igneous state. M. Vogelsang has discovered that the volcanic rocks present what has been called the "fluidal structure," a structure resulting from the disposition of minute crystals disseminated throughout the vitreous mass, and surrounding the larger crystals which have been previously formed in the lava. This fluidal structure is found in the porphyries, and proves their igneous origin. But on examining the siliceous deposits of the Geyser, M.Vogt found this same structure, and thus it does not belong exclusively to the igneous rocks, but also to those of aqueous origin, provided that they have been in a viscous state. In his study of volcanic rocks, M. Vogt has discovered that the trachytes, the basalts, and the lavas, present common characteristics.

M. Lebert brought under the notice of the section a magnificent series of specimens of amber, and expounded the results of his researches on that substance. The fluorescence of petroleum may be taken as a type of the same phenomenon in amber. For naturalists the most interesting of M. Lebert's specimens are fragments of the conifers which produced the amber, a piece enclosing a movable air-bubble in a drop of water, and a great number of other pieces enclosing insects in a perfect state of preservation.

M. François Forel exhibited a photograph of the fossil man of Mentone, which represents him in the position in which he was found. It would appear that this man was

not buried under a landslip, but that he must have been interred by those who survived him. It is argued that, because it is very unusual to inter the dead in a dwelling for the living, we may conclude that this individual be longed to a nomad horde of the age of the reindeer, who did not inhabit the cavern, but passed it from time to time, and who buried this man in the place where he died. We may mention here that in the Zoological section Dr. Vonga read a paper on the same subject, he having been present at the exhumation of the body. He described the caves, and pointed out their probable mode of formation. The body lay upon its left side in the posi tion of sleep. It showed a circular crack at the base of the skull, the thorax being broken at one place; the remainder is in perfect preservation. The cranium is very fine, all the teeth being preserved; the lower jaw is long, but the angle between the horizontal and the ascending branches is a right angle. Dr. Vonga attributed the remarkable preservation of the body to the properties of the pulverised earth which covered it.

Several members presented to the section their studies of various parts of the Alps, and M. E. Favre read a paper on a section of the Caucasus. In the centre of the latter chain a granitic formation is found. On the two sides paleozoic schists are presented, analogous to those of Grätz, and connected by veins of crystalline schist. They are less developed on the north side than on the other. Upon the northern slope the Secondary and Tertiary formations are in a very normal position, and have but little inclination; upon the other slope, on the contrary, there are many zones of eruptive rocks, and the Secondary formations are less disturbed. M. Favre also spoke to the section on the lower limit of eternal snow and the glacial phenomena which he has observed in this chain.

In the section of Zoology Prof. C. Vogt presented the results of his researches upon the Phyllopodes, especially the Branchiopods and the Artemia.

M. Vogt confirmed the observation of M. Joly, that among the Artemia collected at Cette during the months of July and August, no males were found, and that the females reproduced by parthenogenesis. This fact is so much the more singular that large numbers of males are found in other salt marshes inhabited by the same or analogous species.

M. Auguste Forel presented to the section some curious and interesting results of his researches into the nature and habits of ants. Different communities of ants, even when they are of the same species, are enemies to each other. A single community of ants may possess many nests, which are connected with each other by galleries and tunnels. A community of ants may be either simple or mixed; it is simple when it belongs to a single species, mixed when it belongs to two or more species living on good terms among themselves. There are in each com munity, at one time at least, workers, some males and females. If we consider the mixed communities, we can distinguish, amongst others, slave-ants, obtained by the workers of one species pillaging the ant-hills of another species, and carrying off the cocoons. These, when once hatched, become the auxiliary workers and friends of their captors, doubtless believing that they are of the same origin. The mixed community contains the three sexes of the species who plundered, but only the workers of the species pillaged.

The only paper apparently of importance in the Botanical Section was by Dr. Müller, of Geneva, on a new species of Loranthus from the Philippine Islands, which, from the position of the flowers, presents some very extraordinary but not yet well-established peculiarities.

Other papers of value were read in the various sections, and, considering that the meeting lasted only three days, the amount of work gone through appears extraordinary; but then no mention is made of any excursions.

ON THE WYANDOTTE CAVE AND ITS
FAUNA *

THE

HE Wyandotte Cave traverses the St. Louis Limestone of the Carboniferous formation in Crawford County, in South-Western Indiana. I do not know whether its length has ever been accurately determined, but the proprietors say that they have explored its galleries for twenty-two miles, and it is probable that its extent is equal to that of the Mammoth Cave in Kentucky. Numerous galleries which diverge from its known courses in all directions have been left unexplored.

The Wyandotte Cave is as well worthy of popular favour as the Mammoth. It lacks the large bodies of water which diversify the scene in the latter, but is fully equal to it in the beauty of its stalactites and other ornaments of calcyte and gypsum. The stalactites and sta

has been originally more fractured or fragile than elsewhere, and has given way at times of disturbance, piling masses on the floor. The destruction having reached the thin-bedded strata above, the breaking down has proceeded with greater rapidity, each bed breaking away over a narrower area than that below it. When the heavily-bedded rock has been again reached, the breakage has ceased, and the stratum remains as a heavy coping stone to the hollow dome. Of course the process piles a hill beneath, and the access of water being rendered more

[blocks in formation]
[ocr errors][merged small][merged small][merged small][merged small][merged small][merged small][merged small]

FIG. 7.

FIG. 8.

lagmites are more numerous than in the Mammoth, and the former frequently have a worn, or maccaroni-like form, which is very peculiar. They twist and wind in masses like the locks of Medusa, and often extend in slender runners to a remarkable length. The gypsum rosettes occur in the remote regions of the cave, and are very beautiful. There are also masses of amorphous Brebomaster flavescens.-Fig. 7: Male organ from below. Fig. 8: The gypsum of much purity. The floor in many places is covered with curved branches, and, what is more beautiful, of perfectly transparent acicular crystals, sometimes mingled with imperfect twin-crystals. The loose crystals in one place are in such quantity as to give the name of "Snow Banks" to it. In other places it takes the form of japanning on the roof and wall rock.

In one respect the cave is superior to the Mammothin its vast rooms, with step-like domes, and often huge stalagmites on central hills. In these localities the rock Reprinted from the American Naturalist, to the kindness of the editor of which journal we are also indebted for the loan of the cuts.

same; magnified 7'6 times.

the summit. There is no room in the Mammoth Cave equal to these two.

*An examination into the life of the cave shows it to have much resemblance to that of the Mammoth. The following is a list of sixteen species of animals which I obtained, and by its side is placed a corresponding list of the species obtained by Mr. Cooke and others, at the Mammoth Cave. These number seventeen species. As the Mammoth has been more frequently explored, while two days only were devoted to the Wyandotte, the large

[blocks in formation]

The blind fish of the Wyandotte Cave is the same as that of the Mammoth, the Amblyopsis spelaus DeKay. It must have considerable subterranean distribution, as it has undoubtedly been drawn up from four wells in the neighbourhood of the cave. Indeed, it was from one of these, which derives its water from the cave, that we procured our specimens. We descended a well to the water, some twenty feet below the surface, and found it to communicate by a side opening with a long low channel, through which flowed a lively stream of very cold water. Wading up the current in a stooping posture, we soon reached a shallow expansion or pool. Here a blind crawfish was detected crawling round the margin, and was promptly consigned to the alcohol bottle. A little farther beyond, deeper water was reached, and an erect position became possible. We drew the seine in a narrow channel, and after an exploration under the bordering rocks, secured two fishes. A second haul secured another. Another was seen, but we failed to catch it, and on emerging from the cave I had a fifth securely in my hand, as I thought, but found my fingers too numb to prevent its freeing itself by its active struggles.

If these Amblyopses be not alarmed, they come to the surface to feed, and swim in full sight like white aquatic ghosts. They are then easily taken by the hand or net, if perfect silence is preserved, for they are unconscious of the presence of an enemy except through the medium of hearing. This sense is, however, evidently very acute, for at any noise they turn suddenly downward and hide beneath stones, &c., on the bottom. They must take much of their food near the surface, as the life of the depths is apparently very sparse. This habit is rendered easy by the structure of the fish, for the mouth is directed partly upwards, and the head is very flat above, thus allowing the mouth to be at the surface. It thus takes food with less difficulty than other surface feeders, as the perch, &c., where the mouth is terminal or even inferior; for these require a definite effort to elevate the mouth to the object floating on the surface. This could rarely be done with accuracy by a fish with defective or atrophied visual organs. It is therefore probable that fishes of the type of

the Cyprinodontida, the nearest allies of the Hypsarida, and such Hypside as the eyed Chologaster, would possess in the position of the mouth a slight advantage in the struggle for existence.

The blind crawfish above mentioned is specifically distinct from that of the Mammoth Cave, though nearly related to it. I call it Orconectes inermis, separating it generically from Cambarus, or the true crawfishes, on account of the absence of visual organs. The genus Orconectes, then, is established to include the blind crawfishes of the Mammoth and Wyandotte Caves.

Dr. Packard has described an interesting genus of Isopoda allied to the marine form Idotea, which Mr. Cooke discovered in a pool in the Mammoth Cave. He called it Cæcidotea. I obtained a second species in a cave adjoining the Wyandotte which differs in several important respects. I call it Cæcidotea microcephala. Both species are blind. The new species is pure white. It was quite active, and the females carried a pair of egg-pouches full of eggs. The situation in which we found it was peculiar. It was only seen in and near an empty log trough used to collect water from a spring dripping from the roof of one of the chambers.

The Lernaan, Cauloxenus stygius Cope, is a remarkable creature. It is a parasite on the blind fish, precisely as numerous species near of kin attach themselves to various species of marine fishes. The Wyandotte species is not so very unlike some of these. It is attached by a pair of altered fore-limbs, which are plunged into the skin of the host, and held securely in that position by the barbed or recurved claws. No parasitic male was observed in the neighbourhood of the female, and it is probable that, as in the other Lernæopodide, he is a free swimmer, and extremely small. The difficulty of finding his mate on an active host-fish must be augmented by the total darkness of his abode, and many must be isolated owing to the infrequent and irregular occurrence of the fish, to say nothing of the scarceness of its own species.

The allied genera, Achtheres and Lernæopoda, present very distinct distributions, the former being fresh water and the latter marine. Lernæopoda is found in the most varied types of fishes and in several seas; Achtheres has been observed on perch from Asia and Europe, and on a South American Pimelodus. It is to the latter that Cauloxenus is most nearly allied, and from such a form we may, perbaps, trace its descent; modification being consequent on its wandering into subterranean streams. The character which distinguishes it from its allies is one which especially adapts it for maintaining a firm hold on its host, i.e., the fusion of its jaw-arms into a single stem.

Whether the present species shared with the Amblyopsis its history and changes, or whether it seized upon the fish as a host at some subsequent period, is a curious speculation. Its location at the mouth of the fish could scarcely be maintained on a species having sight; for if the host did not remove it, other individuals would be apt to.

I may here allude to another blind Crustacean which I took in the Mammoth Cave, and which has been already mentioned in the Annals and Magazine of Natural His tory as a Gammaroid. Mr. Cooke and myself descended a hole, and found, a short distance along a gallery, a clear spring, covering, perhaps, an area ten feet across. Here Mr. Cooke was so fortunate as to procure the Cæcidoten stygia, while I took the species just mentioned, and which I name Stygobromus vitreus. The genus is new, and represents in a measure the Niphargus of Schiödte found in the caves of Southern Europe. This genus has several species in fresh waters, which are of small size, and swin actively, turning on one side or the other.

Of Insects I took four species of beetles, all new to science; two of them of the blind carnivorous genus Anopthhalmus, and two Staphylinida, known by their very short wing-cases and long, flexible abdomen. Dr. George H. Horn has kindly determined them for me.

[merged small][merged small][ocr errors][merged small][merged small][merged small][merged small][merged small][merged small][merged small]

And another Alæocharyde Staphylinide, allied to Tachyusa, also from Wyandotte Cave. No names have as yet been given to any of these, excepting the second. A monograph of Catops has already appeared containing many species from our fauna; and as the work is inaccessible at present, I have hesitated to do more than indicate the presence of the above species.

The cricket of the Wyandotte Cave is stouter than that of the Mammoth, and thus more like the Raphidophora lapidicola of the forest. There were three species of flies, one or more species of Poduridæ, and a Campodea not determined.

Centipedes are much more abundant in the Wyandotte than in the Mammoth Cave. They especially abounded on the high stalagmites which crown the hill beneath the Mammoth dome, which is three miles from the mouth of the cave. The species is quite distinct from that of the Mammoth Cave, and is the one I described some years ago from caves in Virginia and Tennessee. I call it Spirostrephon cavernarum, agreeing with Dr. Packard that the genus Pseudotremia, to which it was originally referred, is of doubtful validity. The allied form found by Mr. Cooke in the Mammoth Cave has been described by Dr. Packard as Spirostrephon Copei. It is eyeless, and is, on this account alone, worthy of being distinguished generically from Spirostrephon. This genus may be then named Scoterpes. I look for the discovery of S. cavernarum in the Mammoth Cave.

Two species of Arachnidans were observed, one a true spider, the other related to the "long-legs" of the woods. A species similar to the former is found in the Mammoth Cave, and others in other caves, but in every instance where I have obtained them they have been lost by the dissolution of their delicate tissues in the impure alcohol. The other forms are more completely chitinised, and are easily preserved; they are related to the genus Gonyleptes, found under stones in various portions of the country. Dr. Wood describes a species from Texas, and I have taken them in Tennessee and Kansas. In the Wyandotte Cave I found a number of individuals of a new species, at a place called the screw-hole. Though living at a distance of four or five miles from the mouth of the cave, this species is furnished with eyes. This species is described as Erebomaster flavescens Cope. In its relationships it may be said to stand between Acanthocheir and Gonyleptes.

Besides Acanthocheir, another blind Gonyleptid exists in the Mammoth Cave, which I found several miles from the mouth. It is blind like the former, but differs in having many more joints to the tarsi, approaching thus the true Phalangia, or long-legs.

Dr. Packard and Mr. Putnam have already discussed the question of the probability of the origin of these blind cave animals by descent from out-door species having eyes. I have already expressed myself in favour of such view, and deem that in order to prove it we need only

establish two or three propositions. First, that there are eyed genera corresponding closely in other general characters with the blind ones; second, that the condition of the visual organs is in some cave type variable; third, if the abortion of the visual organs can be shown to take place coincidently with general growth to maturity, an important point is gained in explanation of the modus operandi of the process.

First, as to corresponding forms; the Typhlichthys of the Mammoth is identical with Chologaster, except in its lack of eyes. Orconectes bears the same relation to Cambarus; Stygobromus bears nearly the same to Gammarus; and Scoterpes is Spirostrephon without eyes and no pores.

Secondly, as to variability. I have already shown that in Gronias nigrilabris, the blind Silurid from the Conestoga in Pennsylvania, while all of several specimens observed were blind, the degree of atrophy of the visual organs varies materially, not only in different fishes, but on different sides of the same fish. In some the corium is imperforate, in others perforate on one side, in others on both sides, a rudimental cornea being thus present. In some the ball of the eye is oval, and in others collapsed. This fish is related specifically to the Amiurus nebulosus of the same waters, more nearly than the latter is to certain other Amiuri of the Susquehanna river basin to which the Conestoga belongs, as for instance the A. lynx; it may be supposed to have been enclosed in a subterranean lake for a shorter time than the blind fishes of the Western Caves, not only on account of the less degree of loss of visual organs, but also in view of its very dark colours.

Thirdly, it is asserted that the young Orconectes possess eyes, and that perhaps those of the Typhlichthys do also. If these statements be accurate, we have here an example of what is known to occur elsewhere, for instance, in the whalebone whales. In a foetal stage these animals possess rudimentary teeth like other Cetacea, which are subsequently absorbed. This disappearance of the eyes is regarded with reason by Prof. Wyman as evidence of the descent of the blind forms from those with visual organs. I would suggest that the process of reduction illustrates the law of "retardation," accompanied by another phenomenon. Where characters which appear latest in embryonic history are lost, we have simple retardation— that is, the animal in successive generations fails to grow up to the highest point, falling farther and farther back, thus presenting an increasingly slower growth in this special respect. Where, as in the presence of eyes, we have a character early assumed in embryonic life, the retardation presents a somewhat different phase. Each successive generation, it is true, fails to come up to the completeness of its predecessor at maturity, and thus exhibits "retardation;" but this process of reduction of rate of growth is followed by its termination in the part long before growth has ceased in other organs. This is an exaggeration of retardation. Thus the eyes in the Orconectes probably once exhibited at maturity the incomplete characters now found in the young, for a long time a retarded growth continuing to adult age before its termination was gradually withdrawn to earlier stages. Growth ceasing entirely, the phase of atrophy succeeded, the organ became stationary at an early period of general growth, being removed, and its contents transferred to the use of other parts by the activity of "growth force." Thus, for the loss of late assumed organs we have "retardation," but for that of early assumed ones, “retardation and atrophy."

The mutual relations of this cave life form an interesting subject. In the first place, two of the beetles, the crickets, the centipede, the small crustaceans (food of the blind fish) are more or less herbivorous. They furnish food for the spiders, crawfish, Anophthalmus, and the fish. The vegetable food supporting them is in the first place fungi which, in various small forms, grow in damp

« ПредыдущаяПродолжить »